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Chemistry, Raman and infrared spectroscopic characterization of the phosphate mineral reddingite: (MnFe)3(PO4)2(H2O,OH)3, a mineral found in lithium-bearing pegmatite
Authors:Ray L. Frost  Yunfei Xi  Ricardo Scholz  Fernanda M. Belotti  Leonardo E. Lagoeiro
Affiliation:1. Science and Engineering Faculty, School of Chemistry, Physics and Mechanical Engineering, Queensland University of Technology, GPO Box 2434, Brisbane, QLD, 4001, Australia
2. Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG, 35400-00, Brazil
3. Federal University of Itajubá, Campus Itabira, Itabira, MG, 35903-087, Brazil
Abstract:Detailed investigation of an intermediate member of the reddingite–phosphoferrite series, using infrared and Raman spectroscopy, scanning electron microcopy and electron microprobe analysis, has been carried out on a homogeneous sample from a lithium-bearing pegmatite named Cigana mine, near Conselheiro Pena, Minas Gerais, Brazil. The determined formula is $ ({text{Mn}}_{1.60} {text{Fe}}_{1.21} {text{Ca}}_{0.01} {text{Mg}}_{0.01} )_{sum 2.83} ({text{PO}}_{4} )_{2.12} cdot ({text{H}}_{2} {text{O}}_{2.85} {text{F}}_{0.01} )_{sum 2.86} $ , indicating predominance in the reddingite member. Raman spectroscopy coupled with infrared spectroscopy supports the concept of phosphate, hydrogen phosphate and dihydrogen phosphate units in the structure of reddingite-phosphoferrite. Infrared and Raman bands attributed to water and hydroxyl stretching modes are identified. Vibrational spectroscopy adds useful information to the molecular structure of reddingite–phosphoferrite.
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